Interlobate esker architecture and related hydrogeological features derived from a combination of high-resolution reflection seismics and refraction tomography, Virttaankangas, southwest Finland; [Architecture et caractéristiques hydrogéologiques associées d’eskers interlobés basées sur une combinaison de sismique réflexion à haute résolution et de tomographie par réfraction, Virttaankangas, Sud-Ouest de la Finlande]; [Arquitetura interlobática de esker e feições hidrogeológicos relacionadas derivadas de uma combinação de sísmica de reflecção de alta resolução e tomografia de refração, Virttaankangas, sudoeste da Finlândia]; [Arquitectura de eskers interlobulares y características hidrogeológicas relacionadas derivada de la combinación de sísmica de reflexión y tomografías de refracción de alta resolución, Virttaankangas, sudoeste de Finlandia]

被引:0
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作者
Maries G. [1 ]
Ahokangas E. [2 ]
Mäkinen J. [2 ]
Pasanen A. [3 ]
Malehmir A. [1 ]
机构
[1] Department of Earth Sciences, Uppsala University, Uppsala
[2] Department of Geography and Geology, University of Turku, Turku
[3] Unit of Industrial Environments and Recycling, Geological Survey of Finland (GTK), Kuopio
关键词
Esker architecture; Finland; Geophysical methods; Landstreamer; Unconsolidated sediments;
D O I
10.1007/s10040-016-1513-9
中图分类号
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摘要
A novel high-resolution (2–4 m source and receiver spacing) reflection and refraction seismic survey was carried out for aquifer characterization and to confirm the existing depositional model of the interlobate esker of Virttaankangas, which is part of the Säkylänharju-Virttaankangas glaciofluvial esker-chain complex in southwest Finland. The interlobate esker complex hosting the managed aquifer recharge (MAR) plant is the source of the entire water supply for the city of Turku and its surrounding municipalities. An accurate delineation of the aquifer is therefore critical for long-term MAR planning and sustainable use of the esker resources. Moreover, an additional target was to resolve the poorly known stratigraphy of the 70–100-m-thick glacial deposits overlying a zone of fractured bedrock. Bedrock surface as well as fracture zones were confirmed through combined reflection seismic and refraction tomography results and further validated against existing borehole information. The high-resolution seismic data proved successful in accurately delineating the esker cores and revealing complex stratigraphy from fan lobes to kettle holes, providing valuable information for potential new pumping wells. This study illustrates the potential of geophysical methods for fast and cost-effective esker studies, in particular the digital-based landstreamer and its combination with geophone-based wireless recorders, where the cover sediments are reasonably thick. © 2016, The Author(s).
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页码:829 / 845
页数:16
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